clay and 1-3-dichloro-1-propene

clay has been researched along with 1-3-dichloro-1-propene* in 2 studies

Other Studies

2 other study(ies) available for clay and 1-3-dichloro-1-propene

ArticleYear
Sorption of the fumigant 1,3-dichloropropene on soil.
    Journal of environmental science and health. Part. B, Pesticides, food contaminants, and agricultural wastes, 2004, Volume: 39, Issue:4

    The fumigant 1,3-dichloropropene (1,3-D) is considered a major replacement to methyl bromide, which is to be phased out of use in the United States by 2005. The main purpose of this study was to evaluate soil-water partitioning of 1,3-D in two California agricultural soils (Salinas clay loam and Arlington sandy loam). The partition coefficients (Kd and Kf) were determined by directly measuring the concentration of 1,3-D in the solid phase (Cs) and aqueous phase (Cw) after batch equilibration. In the Salinas clay loam, the Kf of cis-1,3-D in adsorption and desorption isotherms was 0.47 and 0.54, respectively, with respective values of 0.39 and 0.49 for trans-1,3-D. This slight hysteric effect suggests that a different range of forces are involved in the adsorption and desorption process. Since n was near unity in the Freundlich equation, the Freundlich isotherms can also be approximated using the liner isotherm. At 25 degrees C, the Kd of the 1,3-D isomers in both soils ranged from 0.46 to 0.56, and the Koc (organic matter partition coefficient) ranged from 58 to 70. The relatively low Kd values and a Koc that falls within the range of 50-150, suggests that 1,3-D is weakly sorbed and highly mobile in these soils. Understanding the sorption behavior of 1,3-D in soil is important when developing fumigation practices to reduce the movement of 1,3-D to the air and groundwater.

    Topics: Adsorption; Allyl Compounds; Aluminum Silicates; Clay; Fumigation; Hydrocarbons, Chlorinated; Insecticides; Silicon Dioxide; Soil Pollutants; Temperature; Water Pollutants

2004
Formation and extraction of persistent fumigant residues in soils.
    Environmental science & technology, 2003, May-01, Volume: 37, Issue:9

    Fumigants are commonly thought to be short-lived in soil, but residues have been found in soils years following application. In this study, formation and extraction of persistent soil fumigant residues were investigated. Fumigants 1,3-dichloropropene (1,3-D), chloropicrin (CP), and methyl isothiocyanate (MITC) were spiked into Arlington, Glenelg, and Hagerstown soils and incubated for 30 d under controlled conditions. The incubated soils were evaporated for 20 h prior to extraction with a variety of organic solvents at different temperatures. Extraction with acetonitrile in sealed vials at 80 degrees C for 24 h was the most efficient method to recover persistent soil fumigant residues. At application rates of 1000-1700 mg (kg of soil)(-1), persistent residues of 1,3-D, CP, and MITC in the three soils ranged from 5 to 67 mg kg(-1). The residue content increased with application rate, correlated positively with soil silt content, decreased dramatically as indigenous organic matter (OM) was removed, and changed little with external OM addition. Adsorption to clay surfaces was not important in fumigant retention, while pulverization of soil aggregates significantly decreased persistent fumigant residues. The results suggest that persistent fumigant residues are retained in soil intra-aggregate micropores resulting from binding clay flocs and silt particles by humic substances.

    Topics: Adsorption; Allyl Compounds; Aluminum Silicates; Chemical Warfare Agents; Clay; Herbicides; Humic Substances; Hydrocarbons, Chlorinated; Insecticides; Isothiocyanates; Pesticide Residues; Porosity; Soil Pollutants

2003